1454:
the right bank, from which a race fed
Millbridge Mill. The tail race passed under the road, to the west of Mill Bridge, and joined the main channel further downstream. At Stainton Mill, the mill pond was part of the main channel, next to the road. The mill race continued beside the road, while the beck fell over a weir, and looped away to the west around the mill site. The tail race of the mill and the river rejoined downstream of the mill. In 1849, the mill was operated by Greenwoods, who were carding wool, which was then used to produce stockings and blankets. Below Stainton Bridge End Bridge, a long mill race ran across fields to the south west, to reach Viver Mill. The tail race was known as Catch Water, and rejoined the river just above Deepthwaite Bridge. Viver Mill was first recorded in the 13th century as a corn mill, and remained a corn mill until 1950. Although now converted to a house, the water wheel has been retained, as have some of the cruck beams and other features.
1385:. The single arch is made of limestone, and has curved retaining walls. The structure was badly damaged by storms in December 2015, when flood water washed away its apron, causing the canal towpath above to collapse, as well as damaging the southern portal and the wing walls. Restoration cost £2.2 million, of which £1.5 million came from the Heritage Lottery Fund. Other grants came from the Rural Payments Agency, South Lakeland District Council, Cumbria County Council and Kendal Town Council. The three-year repair project was delayed by high river levels during the winters of 2018 and 2019. New concrete wing walls were built, and the stonework was repaired using as much of the original stone as possible, with some new stone where this was not possible.
35:
55:
1326:
1441:. A minor road runs along the east bank of the stream, past Holme Park. The road crosses the beck twice before arriving at Beehive Bridge, on the B6254 road. Strickley Bridge is just a little further to the east, where Strickley Beck passes under the same road, before joining Beehive Beck on its left bank. By the time it joins Stainton Beck on its right bank, it has descended to below the 300-foot (90 m) contour.
1426:
were completed in 1896. The dam is around 30 feet (9.1 m) high, and there is a central overflow section, consisting of three semi-circular sluice openings with mock medieval turrets on either side. A small machinery house is located at the foot of the overflow channel, which has a date stone showing
October 1896. The reservoir is still owned by United Utilities, but is no longer used for domestic water supply.
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carries a stone showing "J.J.T. 1734". The mill machinery was destroyed by a fire in 1927, and although the wheel and turbine were not damaged, the cost of rebuilding was beyond the means of the owner, Mr Parkin. It was converted into a house in the 1970s. The mill race was on the left bank of the beck, and the corn mill was just above
Millhouse Bridge.
1397:, a two-arched bridge crosses the beck. Its core probably dates from the 17th century, but it was rebuilt and widened in the early 1890s. The B6385 road crosses at Rowell Bridge, and on its upstream side, there was a tramway bridge, where the Gatebeck Tramway crossed on its way from Gatebeck gunpowder works on the
1425:
Beehive Beck, the main tributary of
Stainton Beck, rises just below the 850-foot (260 m) contour on Hay Fell. Within a short distance, it enters Fisher Tarn Reservoir, which was built under powers contained in the Kendal Corporation Act 1894. George E Deacon was the engineer for the works, which
1465:
The
Environment Agency measure water quality of the river systems in England. Each is given an overall ecological status, which may be one of five levels: high, good, moderate, poor and bad. There are several components that are used to determine this, including biological status, which looks at the
1372:
Blease Hall is located on the right bank. It dates from the early 1600s and was built for Robert
Bateman. Beehive Beck flows southwards from Fisher Tarn Reservoir, and joins on the left bank, as St Sunday's Beck turns to the south. It briefly turns to the west at the hamlet of Halfpenny, where there
1449:
Stainton Beck has provided power to a number of mills in the past. A corn mill at
Millholme was first recorded in 1310, and it was powered by a water wheel until the First World War, when a turbine was fitted to supplement the wheel. The present mill house was first occupied by the Tarn family, and
1453:
At
Halfpenny, a hamlet that is part of the parish of Stainton, a weir channelled water into a race on the left bank, which fed Yarn Mill. In 1849, Taylor and Company were spinning flax and tow there, as well as producing sacking. A little further south, a dam across the beck created a mill pond on
1380:
As it approaches
Stainton, its name changes to Stainton Beck. A single span packhorse bridge crosses the beck. It dates from the 17th century and is built of coursed limestone rubble with rough limestone coping blocks. Between the parapets, it is 3 feet (0.9 m) wide. A minor road crosses the
1356:, which is on the opposite side of the summit. It is known as St. Sunday's Beck, and flows southwards, passing through an area of woodland called Hutton Park Plantation before turning to the east. Hutton Park is on the right bank, before it turns southwards again. It is crossed by the
1367:
As it approaches the hamlet of
Millholme, it once powered Millholme Mill, and is crossed by Ewbank Lane at Millholme Bridge. The houses are to the south of the bridge. It turns to the west and is crossed by the B6254 road at St Sunday's Bridge, where it turns to the south-west. The
1388:
Just below the aqueduct, the beck is crossed by a minor road, carried by a bridge constructed in the 17th century or possibly the early 18th century. It has a single segmental arch and long sloping parapets. Tom Beck joins on the left bank, the
1518:
Like many waterways in the UK, the chemical status changed from good to fail in 2019, due to the presence of polybrominated diphenyl ethers (PBDE) and mercury compounds, neither of which had previously been included in the assessment.
1477:
The water quality of the Stainton Beck system was as follows in 2019. The data covers St Sunday's Beck and Stainton Beck, as well as Beehive Beck from its source to its confluence with Stainton Beck.
1360:
at Latterhowe Bridge and then by a minor road. Crakehall Gill and Millrigg Gill combine before joining St Sunday's Beck on the left bank, and the stream flows to the east of the small village of
1756:
1550:
1457:
Gill Mill, on Beehive Beck, was recorded in the 13th century. It was a corn mill, but was later used as a marble mill and then a sawmill. It continued in use into the 1920s.
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is a ford. A weir and sluices channelled water to a mill, and the A65 road crosses both the tail leat and the main channel at Mill Bridge. The road to
1805:
1752:
1381:
beck just before it reaches Stainton Aqueduct, constructed by the engineer John Fletcher in 1818 for the opening of the northern section of the
54:
1474:
and fish. Chemical status, which compares the concentrations of various chemicals against known safe concentrations, is rated good or fail.
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The source of the stream is close to the 980-foot (300 m) contour on the western flank of Lambrigg Fell, near the source of
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road. It descends quite quickly, and is then crossed by the new route between the two towns, the
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the Peasey Beck joins Stainton Beck on its left bank, with the combined flows becoming the
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1978:
1935:"Glossary (see Biological quality element; Chemical status; and Ecological status)"
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runs along the right bank, but loops away from it at Mill Cottage and Mill House.
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Beehive Beck continues from the foot of the dam, and passes under the old
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crosses, and Catch Water joins on the right bank. At the hamlet of
1329:
The bridge over Stainton Beck to the north of Stainton Aqueduct
1775:"Dam and machinery house at Fisher Tarn Reservoir (1087288)"
1857:
1855:
1405:. The tramway was horse-drawn, and closed in 1936.
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1543:"Restoration of Stainton Aqueduct is now complete"
1533:History, Topography, and Directory, of Westmorland
1733:"Deepthwaite Bridge over Stainton Beck (1086553)"
1624:"Pack Horse Bridge at the Post Office (1007138)"
1709:"Stainton Bridge over Stainton Beck (1086534)"
194:
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1689:. Canal and River Trust. 21 October 2020.
1340:, England. Its upper reaches are known as
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1541:Nicholson, Savannah (3 November 2020).
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1849:Ordnance Survey, 6 inch map, 1888-1913
1753:"Fisher Tarn Dam, New Hutton, Cumbria"
20:
1905:from the original on 10 October 2022.
1881:from the original on 10 October 2022.
1553:from the original on 5 November 2020.
61:
7:
1923:from the original on 1 October 2022.
1832:from the original on 1 October 2022.
1808:from the original on 1 October 2022.
1759:from the original on 1 October 2022.
1687:"Stainton Aqueduct, Lancaster Canal"
693:B6254 Beehive and Strickley Bridges
69:Location of the mouth within Cumbria
1875:"Viver Watermill bed and breakfast"
1693:from the original on 5 August 2021.
1780:National Heritage List for England
1738:National Heritage List for England
1714:National Heritage List for England
1653:National Heritage List for England
1629:National Heritage List for England
1605:National Heritage List for England
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133: • coordinates
1:
1648:"Stainton Aqueduct (1086532)"
1585:Ordnance Survey, 1:25,000 map
815:site of Yarn Mill, Halfpenny
101:Physical characteristics
39:Stainton Beck framed by the
1006:Stainton Bridge End Bridge
929:Packhorse Bridge, Stainton
245:Source of St Sunday's Beck
174:23.6 km (14.7 mi)
117: • location
2011:
1961:"Stainton Beck Water Body"
1509:14.7 miles (23.7 km)
1466:quantity and varieties of
1403:Milnthorpe railway station
16:Stream in Cumbria, England
1919:. Old Cumbria Gazetteer.
1500:Stainton Beck Water Body
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1033:Mill race to Viver Mill
835:site of Millbridge Mill
1965:Catchment Data Explorer
1939:Catchment Data Explorer
1917:"Gill Mill, New Hutton"
1600:"Blease Hall (1312207)"
1547:The Westmorland Gazette
591:site of Millholme Mill
272:Source of Beehive Beck
1877:. BedandBreakfast.uk.
1825:. Fine & Country.
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909:site of Stainton Mill
299:Fisher Tarn Reservoir
1967:. Environment Agency.
1798:"Fisher Tarn, Kendal"
1328:
1941:. Environment Agency
1898:. Fine and Country.
1755:. Historic England.
1530:Mannex, P J (1849).
1336:is a watercourse in
1229:B6385 Rowell Bridge
1536:. Simpkin Marshall.
1175:Deepthwaite Bridge
151: /
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1097: A591
986:Stainton Aqueduct
523:site of Gill Mill
390: A684
360:Latterhowe Bridge
356: A684
155:54.2245°N 2.7407°W
1995:Beck watercourses
1985:Rivers of Cumbria
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1486:Ecological status
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1864:, p. 280.
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1468:invertebrates
1461:Water quality
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795:Beehive Beck
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24:Stainton Beck
22:
19:
1964:
1955:
1943:. Retrieved
1938:
1929:
1911:
1893:"Viver Mill"
1887:
1869:
1814:
1801:
1778:
1765:
1747:
1736:
1723:
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1681:
1669:
1659:28 September
1657:. Retrieved
1651:
1638:
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1532:
1523:Bibliography
1517:
1476:
1464:
1456:
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1448:
1428:
1424:
1421:Beehive Beck
1407:Ackenthwaite
1387:
1379:
1366:
1351:
1341:
1333:
1332:
1155:Catch Water
862:Mill Bridge
18:
1862:Mannex 1849
1472:angiosperms
1399:Peasey Beck
1395:Deepthwaite
1257:Peasey Beck
1128:Viver Mill
158: /
1979:Categories
1560:References
1495:Catchment
1415:River Bela
1411:Milnthorpe
1362:New Hutton
1279:River Bela
143:54°13′28″N
126:Milnthorpe
122:River Bela
1503:Moderate
1439:A684 road
1391:A590 road
1358:A684 road
1067:Tom Beck
146:2°44′27″W
1921:Archived
1900:Archived
1879:Archived
1827:Archived
1806:Archived
1757:Archived
1691:Archived
1551:Archived
1435:Sedbergh
1375:Stainton
78:Location
1483:Section
1338:Cumbria
1101:bridge
949:bridge
659:bridge
625:bridge
489:bridge
421:bridge
394:bridge
326:bridge
95:Cumbria
86:England
83:Country
1945:17 May
1492:Length
1431:Kendal
1348:Course
219:Legend
171:Length
111:
91:County
1903:(PDF)
1896:(PDF)
1830:(PDF)
1823:(PDF)
1506:Fail
1445:Mills
107:Mouth
1947:2017
1661:2021
1409:and
1433:to
1401:to
124:at
1981::
1963:.
1937:.
1854:^
1838:^
1804:.
1800:.
1789:^
1777:.
1773:.
1735:.
1731:.
1711:.
1707:.
1650:.
1646:.
1626:.
1622:.
1602:.
1598:.
1568:^
1549:.
1545:.
1470:,
1417:.
1364:.
1344:.
1949:.
1783:.
1741:.
1717:.
1676:.
1663:.
1632:.
1608:.
202:e
195:t
188:v
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